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一次东北冷涡移动过程及其影响分析

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利用自动站观测资料、探空资料及 NCEP 再分析资料,对辽宁地区一次冷涡天气的移动过程及其所造成的影响进行了分析。结果表明,2015年8月2日,辽宁省南部地区出现暴雨天气是在东北冷涡发展成熟阶段产生的,500 hPa 冷涡形势建立与稳定维持为暴雨发生、发展提供了有利的大尺度环流背景;鄂海阻高的稳定维持导致了冷涡的移动缓慢,使得冷暖空气长时间在辽宁省上空交汇。低空急流为暴雨区输送大量不稳定能量、热量以及动量,低层切变线和地面辐合线也为暴雨的触发提供了较好的动力抬升作用。
A Northeast Cold Eddy Movement and Its Impact Analysis
The moving process of a cold eddy weather in Liaoning region and its effect were analyzed, with using data observed by automatic station, sounding data and NCEP reanalysis data. The results showed that heavy rain weather in Southern Liaoning Province on August 2th, 2015 was produced in matured stage from the development of the northeast cold eddy . The establish-ment and steady of 500 hPa cold eddy provided favorable large scale circulation background for storm development . The maintain and stable of Hubei high sea resistance led to the cold eddy moves slowly, and made a long time intersec-tion of warm and cool air in Liaoning Province . Low level jet deliveried a lot of unstable energy, heat and momen-tum for heavy rain area . Low-rise shear line and ground convergence line also provided a good dynamic lifting effect for the heavy rains triggered .

The northeast cold eddyLow level jetConvergence

刘多文、隋明、李俊乐、全美兰、赵思文、赵宇、李祥明、宁大可、亢云龙、王磊、米雷、葛权哲

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辽宁省抚顺市气象台,辽宁抚顺 113006

辽宁省抚顺市清原满族自治县气象局,辽宁抚顺 113300

东北冷涡 低空急流 辐合

2015

农业灾害研究

农业灾害研究

影响因子:0.451
ISSN:1004-7395
年,卷(期):2015.(12)
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